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Musselshell Creek

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Journal Article
Journal: PALAIOS
Published: 01 October 1995
PALAIOS (1995) 10 (5): 424–436.
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1921
AAPG Bulletin (1921) 5 (2): 252–275.
... closed structure on the main Cat Creek axis, where it is crossed by Musselshell river. The Cat Creek anticline proper is shown on Plate I and its relation to the Cat Creek axis is indicated on Plate II which shows the main structural features of the general region. Plate. II. At the present...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1968
AAPG Bulletin (1968) 52 (6): 1033–1041.
... MCFGPD Tiger Ridge   2 Daniels 22-34N-50E Champlin, #1 Foster 1-30 7.818 Lodgepole 6.993 Mission Canyon F 142 B0PD Smoke Creek   3 Liberty 9-34N-4E Pel-Tex, #1 Anderson 10-5 2,696 Madison 1,765 Bow Island F 11,000 MCFGPD Grandview   4 Musselshell 29-10N-31E McAlester Fuel...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1984
AAPG Bulletin (1984) 68 (2): 178–195.
... Montana south of the Musselshell lineament, subsequent to deposition of the Heath Formation and prior to deposition of the Cameron Creek Member, is estimated to have been about 500 m (1,650 ft). That amount of uplift immediately prior to and penecontemporaneous with deposition of the Tyler Formation...
FIGURES | View All (9)
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1949
AAPG Bulletin (1949) 33 (6): 827–836.
... significance as neither of these formations had hitherto been productive in the Rocky Mountain states. Other important discoveries were in the basal Amsden at Big Wall and Melstone in central Montana and in the Hermosa formation at Dove Creek and Boundary Butte in the Four Corners area of Colorado and Utah...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1980
AAPG Bulletin (1980) 64 (3): 316–338.
... is divided into three members—the Virgelle Sandstone Member, 80 to 130 ft (24 to 40 m) thick, and the middle and upper members, which together are as much as 220 ft (67 m) thick. The Eagle Sandstone is underlain by the Telegraph Creek Formation and overlain by the Claggett Shale, both of Late Cretaceous age...
FIGURES | View All (17)
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1962
AAPG Bulletin (1962) 46 (8): 1371–1415.
... waters from the Gulf region invaded the northern Great Plains. As this sea transgressed into Wyoming and Montana, the continental Aptian sands were reworked and redeposited into a blanket type sand called Fall River and First Cat Creek. The Fall River Sandstone has been and still is called Dakota...
FIGURES | View All (25)
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1956
AAPG Bulletin (1956) 40 (6): 1286–1293.
...Herbert D. Hadley; George E. Summers, Jr. ABSTRACT Greatly increased exploratory drilling in Montana resulted in only a slight drop in the success ratio. Development of the Cedar Creek and Poplar fields resulted in increased total production for Montana. A decrease in wildcat drilling in North...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1959
AAPG Bulletin (1959) 43 (2): 329–349.
... dome where the lower 71 feet remain. Rocks belonging to the Devils Pocket formation have been identified in the subsurface in Pole Creek anticline ( Fig. 1 ) where they are only 18 feet thick, in Box Elder dome where they are 38 feet thick, and in the Melstone area in eastern Musselshell County where...
FIGURES | View All (4)
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1922
AAPG Bulletin (1922) 6 (2): 144–150.
... is mined near Sand Springs and which is conspicuously developed along the west side of the Musselshell-Dry divide and around Chalk Butte, near the head of Snow Creek. A s similar dirty coal bed, probably the same bed, is exposed in the bluffs of Dry Creek just east of Van Norman. The thickness of the Lebo...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1956
AAPG Bulletin (1956) 40 (5): 1001–1004.
.... In undisturbed sections the bed of bentonite is ordinarily about 3 feet thick. It is present over the north-central part of Montana from Glacier National Park southeastward to the Missouri River near Wolf Creek and eastward across the Sweetgrass arch at least as far as the Musselshell River (Cobban, 1951a, pp...
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1957
AAPG Bulletin (1957) 41 (6): 1222–1230.
... (2,658,161), Elk Basin (2,007,147), Cabin Creek (1,669,924), Sumatra (1,462,618), Kevin-Sunburst (1,177,270). The Cedar Creek anticline fields, controlled primarily by Shell Oil Company, produced over 7 million bbls. to become the most prolific structure in Montana. The Wolf Springs field in south-central...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1960
AAPG Bulletin (1960) 44 (6): 852–864.
.... Additional development along the Cedar Creek anticline also added a large amount of the increased production. A major project of secondary recovery was initiated this year in the Cat Creek oil field; however, it is expected that the reservoir will not become sufficiently saturated to increase production...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1923
AAPG Bulletin (1923) 7 (5): 488–506.
... development of the Mowry exists in the region from which the Cat Creek fold would drain oil. The Cat Creek anticline is no more favorable structurally than are many other anticlines in Montana, such as Shawmut, Big Elk, Howard Coulee, Big Wall, and Woman’s Pocket, all of which are in the Musselshell Valley...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1923
AAPG Bulletin (1923) 7 (1): 1–13.
... interpretation for the uplifted area between the Cat Creek and Devil’s Basin anticlines is that this area represents a horst in the basement rocks, whose northern edge is marked by the abrupt downward slope of the sedimentary rocks forming the northern limb of the Cat Creek anticline and whose southern edge...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1971
AAPG Bulletin (1971) 55 (7): 990–996.
... development drilling is shown in Table 3 . Development drilling at Hilight, Joe Creek (39), SE Chan, Springen Ranch, and Kaye has increased production from these relatively new fields. Table 3. Production Comparisons, Wyoming Fields, 1970 Field No. Wells Dec. 1970 Field Ac. BOPD Ac...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1923
AAPG Bulletin (1923) 7 (2): 159–178.
...-making sandstone. The thickness in this area is 130 to 300 feet. On the west dome of the Cat Creek anticline the thickness of the Eagle is 115 feet, but it thins out very rapidly to the east and is entirely gone a few miles east of Musselshell River. The Eagle-Virgelle becomes thinner from west...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1977
AAPG Bulletin (1977) 61 (8): 1346–1355.
... sandstone. The Shannon discoveries ( Table 1 , nos. 2, 14, 23, 24) are located south and east of existing Shannon fields, and have caused sustained high exploration and development interest in these directions. Both the Sussex sandstone discoveries (nos. 13, 15) are now in the House Creek West field...
FIGURES
Image
—Microphotographs illustrating early stages in cementation of arenites and ...
Published: 01 January 1972
of Fort Union Formation, Paleocene; Musselshell County, Montana.) Early stage of clay bond to quartz grain in subwacke framework. Note corroded margin of quartz and tendency for some clay minerals to have become attached to irregular surfaces (arrow). Black area ( p ) is largely open pore into which
Journal Article
Published: 01 January 2007
Rocky Mountain Geology (2007) 42 (2): 67–94.
... shales. In Montana, D. bassleri occurs in the Virgelle Sandstone in Glacier County; the Telegraph Creek Formation in Blaine, Toole, Pondera, Teton, Petroleum, Musselshell, Yellowstone, and Big Horn Counties; the Marias River Shale in Toole, Liberty, and Garfield Counties; the Cody Shale in Carbon...
FIGURES | View All (16)